Glaciers are massive, slow-moving rivers of compacted ice that carve striking topographical features across Earth’s high-latitude and high-altitude regions. Divided broadly into alpine glaciers and continental ice sheets, these dynamic agents reshape landscapes through powerful erosional mechanisms like plucking and abrasion. As ice advances and retreats, it leaves behind distinctive erosional forms such as U-shaped valleys, cirques, and hanging valleys along with depositional landforms like moraines, drumlins, and eskers. Mastering glacial geomorphology is essential for understanding Earth’s climatic history, past ice ages, and surface landscape evolution.
Glaciers and Glacial Landforms MCQs
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Correct Answer: b) A large mass of perennial ice resting on land or floating shelf-like in the sea adjacent to land, formed from the accumulation and recrystallization of snow
Explanation:
A glacier is a persistent body of dense ice that is constantly moving under its own weight, formed where the accumulation of snow exceeds its ablation over many years.
Correct Answer: b) Névé or Firn
Explanation:
Firn (or névé) is granular snow, especially on the upper part of a glacier, that has not yet been compressed into solid ice but has survived a season of melting.
Correct Answer: b) 10%
Explanation:
Today, glaciers and ice sheets cover about 10% of the Earth's land area, primarily in Antarctica and Greenland.
Correct Answer: c) Ice sheet
Explanation:
An ice sheet is a mass of glacier ice that covers surrounding terrain and is greater than 50,000 square kilometers. Only two exist today: the Antarctic and Greenland ice sheets.
Correct Answer: b) Piedmont glacier
Explanation:
Piedmont glaciers form when steep valley glaciers spill into relatively flat plains, spreading out into bulb-like lobes.
Correct Answer: a) Tidewater glaciers
Explanation:
Tidewater glaciers are valley glaciers that flow far enough to reach the ocean, where they calve icebergs into the sea.
Correct Answer: b) Equilibrium line
Explanation:
The equilibrium line (or snowline) marks the area where annual accumulation of snow perfectly balances the annual ablation (melting and sublimation).
Correct Answer: c) It will advance
Explanation:
A positive mass balance (accumulation > ablation) causes the glacier to grow, pushing its terminus further down-valley (advancing).
Correct Answer: b) Sublimation
Explanation:
Sublimation is a component of ablation where ice turns directly into vapor, commonly occurring in cold, dry, high-altitude environments.
Correct Answer: b) Plastic deformation
Explanation:
Below roughly 50 meters, the pressure from overlying ice is immense, causing the ice to behave plastically and flow rather than break.
Correct Answer: b) Basal sliding
Explanation:
Basal sliding occurs when meltwater acts as a lubricant between the glacier's base and the underlying bedrock, allowing the ice mass to slide.
Correct Answer: c) Zone of fracture
Explanation:
Because there is less pressure near the surface, the top 50 meters of ice behaves like a brittle solid, fracturing under stress to form crevasses.
Correct Answer: c) Crevasse
Explanation:
Crevasses are deep fissures that form in the zone of fracture due to tensional stress as the glacier moves over uneven terrain.
Correct Answer: b) Bergschrund
Explanation:
A bergschrund is a large, often deep crevasse that forms where the active, moving glacier ice pulls away from the stagnant ice attached to the mountain.
Correct Answer: b) A short-lived event where a glacier advances at velocities up to 100 times normal
Explanation:
Surge-type glaciers experience periodic phases of extremely rapid flow, often triggered by changes in subglacial hydrology and water pressure.
Correct Answer: b) Ogives
Explanation:
Ogives are wave-like bands on the glacier surface that typically form at the base of icefalls, representing seasonal differences in flow and accumulation.
Correct Answer: b) Plucking (quarrying)
Explanation:
Plucking occurs when meltwater enters cracks in the bedrock, freezes, and attaches the rock to the glacier. As the glacier moves, it plucks the rock away.
Correct Answer: b) Abrasion
Explanation:
Abrasion is the scouring and grinding of bedrock by rocks and debris carried in the basal layers of the moving glacier.
Correct Answer: c) Glacial striations
Explanation:
Glacial striations are parallel scratches carved into bedrock by rocks dragged along the base of the glacier, indicating the direction of ice flow.
Correct Answer: b) Rock flour
Explanation:
Rock flour is the extremely fine-grained, silt-sized powder created by the grinding action of glacial abrasion. It often gives glacial lakes a milky turquoise color.
Correct Answer: b) Chatter marks
Explanation:
Chatter marks (or crescentic gouges) are series of semi-circular or crescent-shaped fractures chipped out of bedrock by irregular rolling or dragging of subglacial boulders.
Correct Answer: b) U-shaped
Explanation:
While rivers carve V-shaped valleys, glaciers erode both the bottom and sides of the valley, creating steep-walled, flat-bottomed U-shaped valleys (glacial troughs).
Correct Answer: b) Hanging valley
Explanation:
Main glaciers erode deeper than smaller tributary glaciers. When the ice melts, the tributary valleys are left 'hanging' above the main valley, often forming waterfalls.
Correct Answer: c) Paternoster lakes
Explanation:
Paternoster lakes are a series of step-like glacial lakes in a U-shaped valley, resembling the beads of a rosary.
Correct Answer: c) Fjord
Explanation:
Fjords are steep-sided, narrow inlets of the sea formed when coastal glacial U-shaped valleys are flooded after the ice melts and sea levels rise.
Correct Answer: c) Cirque
Explanation:
A cirque is an erosional basin formed at the origin of a glacier by plucking and frost wedging against the mountain wall.
Correct Answer: a) Tarn
Explanation:
A tarn is a small, deep lake that occupies an ice-gouged cirque basin.
Correct Answer: a) Arête
Explanation:
An arête is a thin ridge of rock left behind when two parallel glaciers erode their valleys, narrowing the divide between them.
Correct Answer: c) Horn
Explanation:
A horn is a pyramidal peak created by headward erosion of multiple cirques surrounding a single high mountain peak. The Matterhorn is a famous example.
Correct Answer: b) Col
Explanation:
A col is a saddle-like mountain pass created by the intersection of two cirques backing into each other.
Correct Answer: b) Roche moutonnée
Explanation:
A roche moutonnée is an erosional bedrock feature. The glacier smooths the side it hits first (stoss) and plucks chunks from the trailing side (lee).
Correct Answer: b) Crag and tail
Explanation:
A crag and tail forms when a highly resistant rock (crag) shelters softer material (tail) on its leeward side from glacial erosion.
Correct Answer: a) Nunatak
Explanation:
Nunataks are exposed, rocky ridges or peaks not covered with ice or snow within an ice field or glacier.
Correct Answer: c) Trimline
Explanation:
A trimline is a clear boundary on a valley wall representing the highest extent of recent glacial ice, often separating mature vegetation above from scoured rock or younger vegetation below.
Correct Answer: b) Glacial drift
Explanation:
Glacial drift is the comprehensive term for all sediments of glacial origin, which is further subdivided into till and stratified drift.
Correct Answer: c) Till
Explanation:
Till is the direct deposit of glacial ice. Because ice cannot sort sediment by size the way water does, till is characteristically an unsorted jumble of rock sizes.
Correct Answer: c) Stratified drift
Explanation:
Stratified drift refers to glacial sediments deposited by meltwater. Because flowing water sorts particles by size, these deposits are layered (stratified).
Correct Answer: b) Glacial erratic
Explanation:
Glacial erratics are rocks carried far from their source by glacial ice. They stand out because their lithology does not match the local bedrock.
Correct Answer: b) Dropstone
Explanation:
Dropstones are deposited when icebergs carrying glacial debris melt in open water, dropping large stones into the fine muddy sediments of the lake or ocean floor.
Correct Answer: c) Terminal (end) moraine
Explanation:
A terminal moraine is a specific type of end moraine that marks the absolute maximum limit of a glacier's advance.
Correct Answer: d) Lateral moraine
Explanation:
Lateral moraines form along the sides of a glacier, consisting of debris scraped from the valley walls and material falling onto the ice.
Correct Answer: a) Medial moraine
Explanation:
A medial moraine is formed when two glaciers meet, and their adjacent lateral moraines combine to form a central ridge of debris carried down-glacier.
Correct Answer: b) Recessional moraine
Explanation:
Recessional moraines are created during pauses in a glacier's retreat, acting as 'pause marks' that show where the terminus temporarily stabilized.
Correct Answer: a) Ground moraine
Explanation:
Ground moraine forms a gently undulating surface of till deposited steadily as the glacier base melts and retreats.
Correct Answer: b) Drumlin
Explanation:
Drumlins are asymmetrical hills of till. The steep side faces the direction from which the ice advanced, and the gentle, tapering side points in the direction of ice flow.
Correct Answer: a) Up-glacier (the direction the ice came from)
Explanation:
In a drumlin, the steep (stoss) side faces up-glacier. In an erosional roche moutonnée, the steep, plucked (lee) side faces down-glacier.
Correct Answer: b) Esker
Explanation:
Eskers are the cast remnants of streams that flowed in tunnels under or within the melting glacier, leaving sinuous ridges of sorted sediment.
Correct Answer: a) Kame
Explanation:
Kames are mounds of sand and gravel formed when meltwater washes sediment into holes or crevasses on stagnant ice. When the ice melts, the sediment slumps into a mound.
Correct Answer: b) Kame terrace
Explanation:
Kame terraces form when streams deposit sediment along the margin of a valley glacier and the rock wall. Once the ice melts, the terrace is left suspended on the valley side.
Correct Answer: b) Kettle
Explanation:
Kettles (or kettle lakes) are steep-sided holes left behind in an outwash plain or moraine after a buried block of glacial ice melts.
Correct Answer: a) Outwash plain
Explanation:
An outwash plain (or sandur) is a wide expanse of sand and gravel deposited by braided meltwater streams flowing away from the terminus of a glacier.
Correct Answer: b) Jökulhlaup
Explanation:
Jökulhlaup is an Icelandic term for a massive glacial outburst flood, which can dramatically alter landscapes in a very short time.
Correct Answer: c) Braided
Explanation:
Glacial outwash streams are usually braided because they are choked with coarse sediment and experience highly variable daily and seasonal discharges.
Correct Answer: b) Loess
Explanation:
Much of the world's loess (such as in the US Midwest) originated as rock flour from glacial outwash plains, which was then picked up and deposited by strong winds.
Correct Answer: a) Proglacial lake
Explanation:
Proglacial lakes form just ahead of the glacier margin, often dammed by the ice itself or by terminal moraines.
Correct Answer: c) Lake Agassiz
Explanation:
Lake Agassiz was an immense proglacial lake formed by meltwater from the retreating Laurentide Ice Sheet.
Correct Answer: b) Pluvial lakes
Explanation:
Pluvial lakes, such as Lake Bonneville (ancestor of the Great Salt Lake), formed far from the ice sheets in the Great Basin due to a cooler, wetter Ice Age climate.
Correct Answer: a) Varves
Explanation:
Varves are rhythmic, alternating layers of silt/sand (summer melt) and clay (winter freeze), allowing geologists to count years of glacial history.
Correct Answer: a) Isostatic rebound
Explanation:
Glacial isostatic adjustment (or rebound) occurs because the immense weight of ice sheets depresses the crust into the mantle. When the ice melts, the crust slowly rises back up.
Correct Answer: b) Pleistocene Epoch
Explanation:
The Pleistocene Epoch spanned from about 2.58 million to 11,700 years ago and is famous for its repeated cycles of glacial advances and retreats.
Correct Answer: c) Laurentide Ice Sheet
Explanation:
The Laurentide Ice Sheet was the primary ice mass over eastern and central North America, profoundly shaping the landscape, including the Great Lakes.
Correct Answer: b) Fennoscandian Ice Sheet
Explanation:
The Fennoscandian Ice Sheet was the massive ice body centered over Scandinavia that scoured northern Europe during the Pleistocene glaciations.
Correct Answer: b) Milankovitch cycles
Explanation:
Milutin Milankovitch identified three cyclical variations in Earth's orbit—eccentricity, obliquity, and precession—that influence solar radiation distribution and trigger glacial cycles.
Correct Answer: c) Obliquity
Explanation:
Obliquity is the tilt of Earth's axis. A smaller tilt results in cooler summers at high latitudes, which prevents winter snow from melting and allows glaciers to grow.
Correct Answer: c) Eccentricity
Explanation:
Eccentricity describes the elliptical nature of Earth's orbit, which dictates the severity of seasonal variations based on Earth's distance from the Sun.
Correct Answer: b) Precession
Explanation:
Axial precession is the wobble of Earth's axis, like a spinning top, changing which hemisphere is pointed at the sun during perihelion and aphelion.
Correct Answer: b) Ice-albedo positive feedback
Explanation:
White ice has a high albedo (reflectivity). As ice expands, more sunlight is reflected rather than absorbed, cooling the planet further and causing more ice to form (a positive feedback loop).
Correct Answer: b) A period of warmer global climate
Explanation:
In ice cores, warmer temperatures provide the energy needed to evaporate the heavier O-18 from the oceans, resulting in higher O-18 levels in the snow that falls on ice sheets during warm periods.
Correct Answer: b) Periglacial
Explanation:
Periglacial environments are characterized by intense freezing and thawing cycles and permafrost, but they are not permanently covered by glacial ice.
Correct Answer: b) Permafrost
Explanation:
Permafrost is a defining feature of periglacial zones, referring specifically to the thermal condition of the ground remaining below freezing for at least two years.
Correct Answer: b) Active layer
Explanation:
The active layer is the highly dynamic, shallow surface layer of soil in a permafrost region that undergoes annual freezing and thawing.
Correct Answer: b) Talik
Explanation:
A talik is a localized area of unfrozen ground in a continuous permafrost area, typically kept liquid by the thermal mass of an overlying water body.
Correct Answer: a) Pingo
Explanation:
Pingos are earth-covered mounds with a solid core of ice. They grow as pressurized groundwater freezes and expands beneath the surface.
Correct Answer: b) Patterned ground
Explanation:
Patterned ground consists of polygons, circles, or stripes of sorted stones formed by frost heaving in periglacial environments.
Correct Answer: b) Gelifluction (Solifluction)
Explanation:
When the active layer thaws in summer, the water cannot penetrate the permafrost below. The waterlogged soil flows slowly downslope in a process called gelifluction (a specific type of solifluction).
Correct Answer: b) Thermokarst
Explanation:
Thermokarst resembles limestone karst but is formed purely by the thermal melting of ground ice, causing the surface to slump into depressions.
Correct Answer: a) Rock glacier
Explanation:
Rock glaciers look like glaciers but are composed primarily of rock fragments held together by ice, flowing very slowly via the deformation of that ice.
Correct Answer: b) Moulin (glacier mill)
Explanation:
A moulin is a roughly circular, vertical to nearly vertical well-like shaft within a glacier through which meltwater enters from the surface.
Correct Answer: b) Cryoconite
Explanation:
Cryoconite is dark, powdery windblown dust (rock, soot, microbes) that absorbs solar radiation and melts small cylindrical holes into the ice surface.
Correct Answer: c) Englacial transport
Explanation:
Englacial transport refers to debris carried within the ice, which often entered through crevasses or was buried by subsequent snowfall.
Correct Answer: c) Supraglacial transport
Explanation:
Supraglacial transport refers to material riding on top of the glacier, usually derived from rockfalls off adjacent valley walls.
Correct Answer: b) Lodgement till
Explanation:
Lodgement till is 'plastered' or smeared onto the underlying bedrock beneath actively advancing ice, resulting in highly compacted, dense sediment.
Correct Answer: c) 120 meters lower than today
Explanation:
Because millions of cubic kilometers of ocean water were locked up in massive continental ice sheets, global sea levels dropped by about 120-130 meters.
Correct Answer: b) During the Neoproterozoic Era, the Earth's surface became entirely or nearly entirely frozen
Explanation:
The Snowball Earth hypothesis suggests that around 600-700 million years ago, runaway ice-albedo feedback caused glaciation to reach the equator.
Correct Answer: c) Experiencing net mass loss and retreating
Explanation:
Due to anthropogenic climate change and global warming, the vast majority of alpine glaciers worldwide have negative mass balances and are retreating.
Correct Answer: b) Oxygen-18 (18O)
Explanation:
During glaciations, lighter Oxygen-16 is locked in ice sheets, leaving the oceans enriched in heavier Oxygen-18, which is then recorded in marine fossils.
Correct Answer: b) Tillite
Explanation:
Tillite is the sedimentary rock formed when glacial till becomes lithified (turned to stone) over geologic time, providing evidence of ancient glaciations.
Correct Answer: c) It shifts to a higher altitude
Explanation:
As temperatures rise, the zone where melting occurs expands upward, forcing the equilibrium line to a higher altitude.
Correct Answer: b) The overall loss of ice and snow from a glacier
Explanation:
Ablation refers to all processes that remove mass from a glacier, including melting, sublimation, calving, and wind erosion.
Correct Answer: b) The breaking off of chunks of ice at the edge of a glacier, forming icebergs
Explanation:
Calving is the mechanical failure of ice at the terminus of a tidewater glacier or ice shelf, resulting in icebergs falling into the water.
Correct Answer: c) Antarctic Ice Sheet
Explanation:
The Antarctic Ice Sheet is the largest single mass of ice on Earth, containing about 60% of all fresh water on the planet.
Correct Answer: b) Melt-out till
Explanation:
Melt-out till forms when stagnant or slow-moving ice melts, allowing the englacial and supraglacial debris to gently drop and accumulate on the ground.
Correct Answer: c) 65 meters
Explanation:
Current estimates suggest that the total melting of the Antarctic and Greenland ice sheets would raise global sea levels by about 65 to 70 meters.
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